The fibrogenic or carcinogenic response to the inhalation of crystalline silica dusts is strictly related to the physicochemical properties of the particles, which, in turn, are mostly determined by the "origin" and the history of the dust. Several physicochemical properties have been reported to modulate silica pathogenicity. None of them simply correlate with the reported toxicity in all the systems used to study silica pathogenicity. This confirms, on the one hand, that several properties are implicated at the same time, and on the other that pathogenicity is the result of a multistage process. There is a general consensus on the key role played by alveolar macrophages in silica-related diseases. For this article the cytotoxicity of a large variety of silicas, including rather unusual forms, with controlled micromorphology and surface properties, has been studied on a mouse monocyte-machrophage tumor cell line successfully employed in previous studies on cristobalite (Fubini et al., 1999). When compared on a per unit surface basis, crystalline silicas were more cytotoxic than amorphous ones, with the notable exception of stishovite, the nonpathogenic crystalline polymorph, with octahedrally coordinated silicon atoms. Among the amorphous ones, a diatomaceous earth and a powdered silica glass exhibited an intermediate toxicity, higher than what was elicited by a pyrogenic silica. In this study a new class of crystalline silicas have been considered, pure-silica zeolites, which constitute a new morphological entity with which cells may be confronted. The cytotoxicity of these samples varies from inert to highly cytotoxic, covering all the range of toxicity covered by the traditional silica dusts. We discuss the influence of morphological properties and surface reactivity on the cytotoxicity of several pure-silica zeolites. The extent of exposed surface and the shape of the particles correlate with cell toxicity. The lower cytotoxicity of one "non-pathogenic quartz" and of an aluminum-coated Min-U-Sil quartz, compared with the original pathogenic Min-U-Sil quartz, suggest a depressive effect of the aluminum ions present at the surface of both quartzes. The extreme variability in the biological response to crystalline silicas is confirmed and a new class of materials is brought to the study of the mechanisms of silica pathogenicity.